This project dated an Early Archaean partial convective overturn (tectonic) event in the East Pilbara Terrane, giving the first direct age for this event. Petrology, geochemistry and geochemistry techniques were combined in an exemplar case study of how to date deformation events in complex, poly-deformational rocks using the accessory mineral titanite
Mineralizing events in the North Pilbara terrain of Western Australia occured between 3490 and 2700 ...
Models for the formation of the high-amplitude (minimum 15 km), long wavelength (120 km) granitoid d...
The Archaean era lasted for about one third of the Earth's history, from ca 4.0 until 2.5 billion ye...
Sensitive high-resolution ion microprobe (SHRIMP) U-Pb dating of zircons from granitic rocks in the ...
The Shaw area in the eastern Pilbara Craton, consists of granitoids with intrusion ages ranging from...
During the early Archaean, the Earth was too hot to sustain rigid lithospheric plates subject to Wil...
The Archaean Pilbara Craton in Western Australia has a domainal architecture which has been interpre...
This thesis examined how the oldest core of the Australian continent formed more than 3.5 billion ye...
The Pilbara Craton, Western Australia, is one of the best preserved Palaeo- to Mesoarchaean terrains...
A palinspastic reconstruction of a 100 km long traverse through Archaean rocks of the East Pilbara, ...
A palinspastic reconstruction of a 100 km long traverse through Archaean rocks of the East Pilbara, ...
The Shaw Granitoid Complex, one of the classic granitoid domes of the Archaean Pilbara Craton, Weste...
The early Archaean East Pilbara Terrane of the Pilbara Craton represents the archetypical granite do...
The global tectonic setting(s) of the early Archean is a long-debated topic in geology. There are tw...
U-Pb ion microprobe analysis of zircon indicates that the oldest rocks from the southern Prince Char...
Mineralizing events in the North Pilbara terrain of Western Australia occured between 3490 and 2700 ...
Models for the formation of the high-amplitude (minimum 15 km), long wavelength (120 km) granitoid d...
The Archaean era lasted for about one third of the Earth's history, from ca 4.0 until 2.5 billion ye...
Sensitive high-resolution ion microprobe (SHRIMP) U-Pb dating of zircons from granitic rocks in the ...
The Shaw area in the eastern Pilbara Craton, consists of granitoids with intrusion ages ranging from...
During the early Archaean, the Earth was too hot to sustain rigid lithospheric plates subject to Wil...
The Archaean Pilbara Craton in Western Australia has a domainal architecture which has been interpre...
This thesis examined how the oldest core of the Australian continent formed more than 3.5 billion ye...
The Pilbara Craton, Western Australia, is one of the best preserved Palaeo- to Mesoarchaean terrains...
A palinspastic reconstruction of a 100 km long traverse through Archaean rocks of the East Pilbara, ...
A palinspastic reconstruction of a 100 km long traverse through Archaean rocks of the East Pilbara, ...
The Shaw Granitoid Complex, one of the classic granitoid domes of the Archaean Pilbara Craton, Weste...
The early Archaean East Pilbara Terrane of the Pilbara Craton represents the archetypical granite do...
The global tectonic setting(s) of the early Archean is a long-debated topic in geology. There are tw...
U-Pb ion microprobe analysis of zircon indicates that the oldest rocks from the southern Prince Char...
Mineralizing events in the North Pilbara terrain of Western Australia occured between 3490 and 2700 ...
Models for the formation of the high-amplitude (minimum 15 km), long wavelength (120 km) granitoid d...
The Archaean era lasted for about one third of the Earth's history, from ca 4.0 until 2.5 billion ye...